Counter-gradient heat transport by large-scale circulation in two-dimensional turbulent convection. (22nd August 2017)

• Record Type: Journal Article
• Authors: Qiang, Wei; Cao, Hui; Li, Weimin; Zhang, Fansiqi
• Is Part Of: Europhysics letters. Volume 118:Number 6(2017:Jun.)
• Publication Date: 2017-08-22
• Subjects: 47.27.te -- 44.25.+f -- 47.27.ek; Physics -- Periodicals; Electronic journals; 530.05
• DOI: 10.1209/0295-5075/118/64001
• Languages: English
• ISSNs: 0295-5075

Abstract

Abstract: We investigate numerically the counter-gradient heat transport in two-dimensional turbulent Rayleigh-Bénard convection, which derives its existence from the descending hot plumes and ascending cold plumes with the large-scale circulation. Both qualitative and quantitative evidence is presented for the Rayleigh numbers from 10 4 to 10 11 and the Prandtl number 1.0 in a domain of aspect ratio 2 with periodic boundary conditions in the horizontal direction. The counter-gradient heat transport increases with Rayleigh numbers, and becomes comparable to the gradient heat transport. The gradient heat transport has a power law dependence on the Rayleigh number with scaling exponent 1/3, while a phase transition of the counter-gradient heat transport can be identified around the critical Rayleigh number . The Reynolds numbers of the gradient and counter-gradient heat transports exhibit identical power law dependence on the Rayleigh numbers with scaling exponent 1/2. The gradient heat transport is partially compensated by the counter-gradient heat transport with increasing Rayleigh numbers, which attenuates the effects of the large-scale circulation on the global heat transfer especially for high Rayleigh numbers. We emphasize that the counter-gradient heat transport also exists in the three-dimensional turbulent Rayleigh-Bénard convection, although the plume and flow structures therein are quite different.